Near Canopy Arctic Acoustic Backscattering Study.

We collected under-ice backscattering data with a low frequency (400 Hz), spatially diverse, transmitting and receiving array during the ONR SIMI project in Spring '94. The experiment, termed IBEX (Ice Backscattering Experiment) was based on the idea that such arrays of sources and receivers ca...

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Main Authors: Ewart, Terry, Henyey, Frank, Olson, Leroy, Williams, Kevin
Other Authors: WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB
Format: Text
Language:English
Published: 1994
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA327295
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA327295
id ftdtic:ADA327295
record_format openpolar
spelling ftdtic:ADA327295 2023-05-15T15:07:48+02:00 Near Canopy Arctic Acoustic Backscattering Study. Ewart, Terry Henyey, Frank Olson, Leroy Williams, Kevin WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB 1994-09 text/html http://www.dtic.mil/docs/citations/ADA327295 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA327295 en eng http://www.dtic.mil/docs/citations/ADA327295 Approved for public release; distribution is unlimited. DTIC Snow Ice and Permafrost Acoustic Detection and Detectors *ACOUSTIC IMAGES *BACKSCATTERING *UNDERICE ACOUSTIC TRACKING ARRAYS ICE MECHANICS INTERFEROMETRY LOW FREQUENCY PULSE TRANSMITTERS RECEIVERS SEA ICE IBEX(ICE BACKSCATTERING EXPERIMENT) Text 1994 ftdtic 2016-02-24T09:18:50Z We collected under-ice backscattering data with a low frequency (400 Hz), spatially diverse, transmitting and receiving array during the ONR SIMI project in Spring '94. The experiment, termed IBEX (Ice Backscattering Experiment) was based on the idea that such arrays of sources and receivers can be used to make images of backscattered sound when the geometry is very well known. The data has been processed using interferometric (time delay) imaging to localize high scattering regions. The measurements were made in two locations; one directed at imaging a large ridge, the other directed at imaging an 1000 m diameter expanse of a single floe. The measurements were carried out using several pulse types. We also operated a hyperbolic noise event tracking system to locate ice-cracking events and initiate an imaging sequence. The noise levels and activity were so low during the experiment period, that this feature could not be utilized. The ridge imaging was a collaborative effort with the MIT Group under the direction of Hendrik Schmidt. We have not received the MIT data for the combined effort at this writing. Text Arctic Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Acoustic Detection and Detectors
*ACOUSTIC IMAGES
*BACKSCATTERING
*UNDERICE
ACOUSTIC TRACKING
ARRAYS
ICE MECHANICS
INTERFEROMETRY
LOW FREQUENCY
PULSE TRANSMITTERS
RECEIVERS
SEA ICE
IBEX(ICE BACKSCATTERING EXPERIMENT)
spellingShingle Snow
Ice and Permafrost
Acoustic Detection and Detectors
*ACOUSTIC IMAGES
*BACKSCATTERING
*UNDERICE
ACOUSTIC TRACKING
ARRAYS
ICE MECHANICS
INTERFEROMETRY
LOW FREQUENCY
PULSE TRANSMITTERS
RECEIVERS
SEA ICE
IBEX(ICE BACKSCATTERING EXPERIMENT)
Ewart, Terry
Henyey, Frank
Olson, Leroy
Williams, Kevin
Near Canopy Arctic Acoustic Backscattering Study.
topic_facet Snow
Ice and Permafrost
Acoustic Detection and Detectors
*ACOUSTIC IMAGES
*BACKSCATTERING
*UNDERICE
ACOUSTIC TRACKING
ARRAYS
ICE MECHANICS
INTERFEROMETRY
LOW FREQUENCY
PULSE TRANSMITTERS
RECEIVERS
SEA ICE
IBEX(ICE BACKSCATTERING EXPERIMENT)
description We collected under-ice backscattering data with a low frequency (400 Hz), spatially diverse, transmitting and receiving array during the ONR SIMI project in Spring '94. The experiment, termed IBEX (Ice Backscattering Experiment) was based on the idea that such arrays of sources and receivers can be used to make images of backscattered sound when the geometry is very well known. The data has been processed using interferometric (time delay) imaging to localize high scattering regions. The measurements were made in two locations; one directed at imaging a large ridge, the other directed at imaging an 1000 m diameter expanse of a single floe. The measurements were carried out using several pulse types. We also operated a hyperbolic noise event tracking system to locate ice-cracking events and initiate an imaging sequence. The noise levels and activity were so low during the experiment period, that this feature could not be utilized. The ridge imaging was a collaborative effort with the MIT Group under the direction of Hendrik Schmidt. We have not received the MIT data for the combined effort at this writing.
author2 WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB
format Text
author Ewart, Terry
Henyey, Frank
Olson, Leroy
Williams, Kevin
author_facet Ewart, Terry
Henyey, Frank
Olson, Leroy
Williams, Kevin
author_sort Ewart, Terry
title Near Canopy Arctic Acoustic Backscattering Study.
title_short Near Canopy Arctic Acoustic Backscattering Study.
title_full Near Canopy Arctic Acoustic Backscattering Study.
title_fullStr Near Canopy Arctic Acoustic Backscattering Study.
title_full_unstemmed Near Canopy Arctic Acoustic Backscattering Study.
title_sort near canopy arctic acoustic backscattering study.
publishDate 1994
url http://www.dtic.mil/docs/citations/ADA327295
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA327295
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
permafrost
Sea ice
genre_facet Arctic
Ice
permafrost
Sea ice
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA327295
op_rights Approved for public release; distribution is unlimited.
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